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Research From Old Dominion, Kent State and USC Scientists Provides Better Understanding of Climate ChangesPosted Nov. 13, 2012
A team of scientists from Old Dominion University, Kent State University and the University of Southern California has identified for the first time a clear 1,500-year cycle in the Arctic Oscillation (AO), the surface atmosphere pressure pattern in the far north that greatly influences weather in the Northern Hemisphere. Led by ODU geological oceanographer Dennis Darby, the team’s findings are featured this week on the prestigious journal Nature Geoscience’s website. Co-authors of the Nature Geoscience article, titled “1,500-Year Cycle in the Arctic Oscillation Identified in Holocene Arctic Sea-Ice Drift,” are Joseph Ortiz, a geological oceanographer from Kent State; Chester Grosch, a physical oceanographer and computer scientist from ODU; and Steven Lund, a geophysicist from USC. The researchers’ study, which was funded by the National Science Foundation, indicates that this natural cycle could be forcing some of the Arctic ice melting and unusual weather experienced recently in the heavily populated northern half of the globe. In a worst-case scenario that Darby described in an interview, the cyclical pressure pattern could combine with manmade climate change to exacerbate severe weather and flooding trends. In the near term, according to Darby, “The implications are that the severe winters of 2009-11 (experienced in northern Europe and elsewhere) might be tame compared to what is possible, based on past swings in the AO.”
Working on a 20-meter-long sediment core raised offshore of Alaska from 1,300 meters water depth, the researchers could detect varying amounts of iron-rich, sand grains ice-rafted from Russia over the last 8,000 years. Darby and his colleagues were able to show through geochemical analysis that some these Russian grains came from the Kara Sea, which is off the northern Russia landmass east of the northern tip of Finland. This is more than 3,000 miles from the core sample site, and the authors say Kara iron grains could have only arrived at the Alaskan coast by drifting in ice. Furthermore, the ice floes would only move from the Kara to offshore Alaska during a strong positive AO conditions.
When the AO index is positive, surface pressure is low in the polar region. This helps the mid-latitude jet stream to blow strongly and consistently from west to east, thus keeping cold Arctic air locked in the polar region. When the AO index is negative, there tends to be high pressure in the polar region, weaker zonal winds, and greater movement of frigid polar air into the populated areas of the middle latitudes.
Measurements taken by instruments in modern times clearly show relatively short-term fluctuations in the AO, with profound impacts on weather and climate. “But how the AO varies during the Holocene (roughly the last 12,000 years) is not well understood,” the authors write in Nature Geoscience.
Darby said that time-series analysis of the researchers’ geochemical record reveals a 1,500-year cycle that is similar to what other researchers have proposed in recent decades, based on scattered findings in paleoclimate records. But he and his colleagues are the first to find a high-resolution indicator of the Arctic record that resolves multidecadal-through-millennial-scale AO cycles, he said.
Researchers aboard the icebreaker USCGC Healy prepare to deploy a piston core near the location off the Alaskan coast where the core in this study was recovered
Researchers Dennis Darby (ODU), Joseph Oritz (Kent State University), and Jens Bishoff (ODU) from left to right, extract an Arctic sediment core from a piston coring device aboard the icebreaker USCGC Healy.
“Our record is the longest record to date to reconstruct the AO and documents that there is millennial scale variability in the AO,” Ortiz said. “The sedimentation rate at our site is also sufficient to statistically differentiate between a 1,000-year cycle and a 1,500-year cycle, which helps us to understand the dynamics of the response of the climate system to external forcing during the Holocene geological period.”
The 1,500-year cycle is distinct from a 1,000-year cycle found in a similarly analyzed record of total solar irradiance, the authors write, suggesting that the longer cycle arises from either internal oscillation of the climate system or as an indirect response to low-latitude solar forcing.
“The AO can remain in a rather strong negative or positive mode for many decades,” the research team writes in the Nature Geoscience article. “When it is positive as suggested by the upswing in the Kara series during the last 200 years, then the additional warmth due to the entrapped Arctic cold air masses during winters could exacerbate the mid-latitude signature of anthropogenic global warming resulting from increased atmospheric CO2. When the AO is strongly negative as seen in the winters of 2009-11, the Northern Hemisphere experiences prolonged intervals of colder than normal conditions. Because the maximum amplitudes of the AO as recorded in the Kara (iron) grain record in recent decades is less than a third of the amplitude in the past, the full range of variability in the AO is not likely recorded in the instrumental records of the last few decades.”
This leads Darby to his near-term forecast: “Thus the AO is potentially capable of much larger swings to positive or negative phases. If so, then these much stronger highs and lows should have greater impact on weather and climate, causing much colder Northern Hemisphere winters during a strong negative AO and milder winters during strong positive AO than seen in the last several hundred years. Such AO positive swings could add to anthropogenic warming causing even more rapid ice melt than has been seen in the last decade.”